[HTML][HTML] Cenozoic uplift and erosion of the Norwegian Barents Shelf–A review
Uplift and erosion are complex phenomena in terms of their governing processes, precise
timing and exact magnitude. The intricate relationship between different geodynamic …
timing and exact magnitude. The intricate relationship between different geodynamic …
Geophysical constraints on the dynamics and retreat of the Barents Sea ice sheet as a paleobenchmark for models of marine ice sheet deglaciation
Our understanding of processes relating to the retreat of marine‐based ice sheets, such as
the West Antarctic Ice Sheet and tidewater‐terminating glaciers in Greenland today, is still …
the West Antarctic Ice Sheet and tidewater‐terminating glaciers in Greenland today, is still …
Widespread methane seepage along the continental margin off Svalbard-from Bjørnøya to Kongsfjorden
Numerous articles have recently reported on gas seepage offshore Svalbard, because the
gas emission from these Arctic sediments was thought to result from gas hydrate …
gas emission from these Arctic sediments was thought to result from gas hydrate …
Postglacial response of Arctic Ocean gas hydrates to climatic amelioration
P Serov, S Vadakkepuliyambatta… - Proceedings of the …, 2017 - National Acad Sciences
Seafloor methane release due to the thermal dissociation of gas hydrates is pervasive
across the continental margins of the Arctic Ocean. Furthermore, there is increasing …
across the continental margins of the Arctic Ocean. Furthermore, there is increasing …
Eurasian Ice Sheet collapse was a major source of Meltwater Pulse 1A 14,600 years ago
Rapid sea-level rise caused by the collapse of large ice sheets is a threat to human
societies. In the last deglacial period, the rate of global sea-level rise peaked at more than 4 …
societies. In the last deglacial period, the rate of global sea-level rise peaked at more than 4 …
Quaternary contourite drifts of the Western Spitsbergen margin
The study of contourite drifts is an increasingly used tool for understanding the climate
history of the oceans. In this paper we analyse two contourite drifts along the continental …
history of the oceans. In this paper we analyse two contourite drifts along the continental …
Spatial changes in gas transport and sediment stiffness influenced by regional stress: Observations from piezometer data along Vestnesa Ridge, eastern Fram Strait
Gas transport through sediments to the seabed and seepage occurs via advection through
pores, faults, and fractures, and as solubility driven gas diffusion. The pore pressure gradient …
pores, faults, and fractures, and as solubility driven gas diffusion. The pore pressure gradient …
Origin of shallow submarine mass movements and their glide planes—Sedimentological and geotechnical analyses from the continental slope off northern Norway
NJ Baeten, JS Laberg, M Vanneste… - Journal of …, 2014 - Wiley Online Library
Submarine landslides are often characterized by a basal surface of rupture parallel to the
stratigraphy, in which downslope movement is initiated. However, little is known about the …
stratigraphy, in which downslope movement is initiated. However, little is known about the …
Exceptions to bed-controlled ice sheet flow and retreat from glaciated continental margins worldwide
Projections of ice sheet behavior hinge on how ice flow velocity evolves and the extent to
which marine-based grounding lines are stable. Ice flow and grounding line retreat are …
which marine-based grounding lines are stable. Ice flow and grounding line retreat are …
Record of methane emissions from the West Svalbard continental margin during the last 23.500 yrs revealed by δ13C of benthic foraminifera
G Panieri, RH James, A Camerlenghi… - Global and Planetary …, 2014 - Elsevier
The values of δ 13 C in benthic foraminifera have been measured in a gas-hydrate-bearing
sediment core collected from an area of active methane venting on the Vestnesa Ridge …
sediment core collected from an area of active methane venting on the Vestnesa Ridge …